First lake record of Holocene climate and vegetation change of the Northern Kuril Islands
Abstract Investigation of Pernatoe Lake sediments in the south of Paramushir Island has enabled us to obtain the first continuous pollen record of climate and vegetation changes in the north of the Kurile archipelago during the Holocene. Series of radiocarbon datings of between 10 000 ± 40 and 2180...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Lozhkin, A. V. [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2010 |
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| Schlagwörter: |
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| Anmerkung: |
© Pleiades Publishing, Ltd. 2010 |
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| Übergeordnetes Werk: |
Enthalten in: Doklady earth sciences - SP MAIK Nauka/Interperiodica, 1998, 430(2010), 2 vom: Feb., Seite 198-200 |
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| Übergeordnetes Werk: |
volume:430 ; year:2010 ; number:2 ; month:02 ; pages:198-200 |
| Links: |
|---|
| DOI / URN: |
10.1134/S1028334X1002011X |
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OLC2040773347 |
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| 100 | 1 | |a Lozhkin, A. V. |e verfasserin |4 aut | |
| 245 | 1 | 0 | |a First lake record of Holocene climate and vegetation change of the Northern Kuril Islands |
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| 520 | |a Abstract Investigation of Pernatoe Lake sediments in the south of Paramushir Island has enabled us to obtain the first continuous pollen record of climate and vegetation changes in the north of the Kurile archipelago during the Holocene. Series of radiocarbon datings of between 10 000 ± 40 and 2180 ± 40 years ago are evidence that the beginning of sediments accumulation, found after borehole development, is related to the Early Holocene. Diatom analysis has shown several stages in the lake development: raised bog on the border of the Pleistocene and Holocene, lagoon formation resulting from the sea level rise over 9–6 ky, and freshwater lake formation 6 ky and up to the present. Climate warming during the period attributed to the boreal and Atlantic periods of the Holocene is reflected by the dominance of Pinus pumila and Alnus serrulata assemblages in vegetation cover. Wide dune fields were formed in the Sea of Okhotsk and the Pacific shores of Paramushir Island 5–4 ky. Strengthening of atmogenic processes is related to cooling of the climate and drying of some areas of the underwater slope. | ||
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| 700 | 1 | |a Cherepanova, M. V. |4 aut | |
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10.1134/S1028334X1002011X doi (DE-627)OLC2040773347 (DE-He213)S1028334X1002011X-p DE-627 ger DE-627 rakwb eng 550 000 VZ 38.00$jGeowissenschaften: Allgemeines bkl 38.55$jRegionale Geologie bkl Lozhkin, A. V. verfasserin aut First lake record of Holocene climate and vegetation change of the Northern Kuril Islands 2010 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Ltd. 2010 Abstract Investigation of Pernatoe Lake sediments in the south of Paramushir Island has enabled us to obtain the first continuous pollen record of climate and vegetation changes in the north of the Kurile archipelago during the Holocene. Series of radiocarbon datings of between 10 000 ± 40 and 2180 ± 40 years ago are evidence that the beginning of sediments accumulation, found after borehole development, is related to the Early Holocene. Diatom analysis has shown several stages in the lake development: raised bog on the border of the Pleistocene and Holocene, lagoon formation resulting from the sea level rise over 9–6 ky, and freshwater lake formation 6 ky and up to the present. Climate warming during the period attributed to the boreal and Atlantic periods of the Holocene is reflected by the dominance of Pinus pumila and Alnus serrulata assemblages in vegetation cover. Wide dune fields were formed in the Sea of Okhotsk and the Pacific shores of Paramushir Island 5–4 ky. Strengthening of atmogenic processes is related to cooling of the climate and drying of some areas of the underwater slope. Holocene Pollen Zone Northern Kuril Island Underwater Slope Gray Siltstone Anderson, P. M. aut Goryachev, N. A. aut Minyuk, P. S. aut Pakhomov, A. Yu. aut Solomatkina, T. B. aut Cherepanova, M. V. aut Enthalten in Doklady earth sciences SP MAIK Nauka/Interperiodica, 1998 430(2010), 2 vom: Feb., Seite 198-200 (DE-627)242069096 (DE-600)1422550-5 (DE-576)079718450 1028-334X nnns volume:430 year:2010 number:2 month:02 pages:198-200 https://doi.org/10.1134/S1028334X1002011X lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_70 38.00$jGeowissenschaften: Allgemeines VZ 106408305 (DE-625)106408305 38.55$jRegionale Geologie VZ 106407260 (DE-625)106407260 AR 430 2010 2 02 198-200 |
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10.1134/S1028334X1002011X doi (DE-627)OLC2040773347 (DE-He213)S1028334X1002011X-p DE-627 ger DE-627 rakwb eng 550 000 VZ 38.00$jGeowissenschaften: Allgemeines bkl 38.55$jRegionale Geologie bkl Lozhkin, A. V. verfasserin aut First lake record of Holocene climate and vegetation change of the Northern Kuril Islands 2010 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Ltd. 2010 Abstract Investigation of Pernatoe Lake sediments in the south of Paramushir Island has enabled us to obtain the first continuous pollen record of climate and vegetation changes in the north of the Kurile archipelago during the Holocene. Series of radiocarbon datings of between 10 000 ± 40 and 2180 ± 40 years ago are evidence that the beginning of sediments accumulation, found after borehole development, is related to the Early Holocene. Diatom analysis has shown several stages in the lake development: raised bog on the border of the Pleistocene and Holocene, lagoon formation resulting from the sea level rise over 9–6 ky, and freshwater lake formation 6 ky and up to the present. Climate warming during the period attributed to the boreal and Atlantic periods of the Holocene is reflected by the dominance of Pinus pumila and Alnus serrulata assemblages in vegetation cover. Wide dune fields were formed in the Sea of Okhotsk and the Pacific shores of Paramushir Island 5–4 ky. Strengthening of atmogenic processes is related to cooling of the climate and drying of some areas of the underwater slope. Holocene Pollen Zone Northern Kuril Island Underwater Slope Gray Siltstone Anderson, P. M. aut Goryachev, N. A. aut Minyuk, P. S. aut Pakhomov, A. Yu. aut Solomatkina, T. B. aut Cherepanova, M. V. aut Enthalten in Doklady earth sciences SP MAIK Nauka/Interperiodica, 1998 430(2010), 2 vom: Feb., Seite 198-200 (DE-627)242069096 (DE-600)1422550-5 (DE-576)079718450 1028-334X nnns volume:430 year:2010 number:2 month:02 pages:198-200 https://doi.org/10.1134/S1028334X1002011X lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_70 38.00$jGeowissenschaften: Allgemeines VZ 106408305 (DE-625)106408305 38.55$jRegionale Geologie VZ 106407260 (DE-625)106407260 AR 430 2010 2 02 198-200 |
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10.1134/S1028334X1002011X doi (DE-627)OLC2040773347 (DE-He213)S1028334X1002011X-p DE-627 ger DE-627 rakwb eng 550 000 VZ 38.00$jGeowissenschaften: Allgemeines bkl 38.55$jRegionale Geologie bkl Lozhkin, A. V. verfasserin aut First lake record of Holocene climate and vegetation change of the Northern Kuril Islands 2010 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Ltd. 2010 Abstract Investigation of Pernatoe Lake sediments in the south of Paramushir Island has enabled us to obtain the first continuous pollen record of climate and vegetation changes in the north of the Kurile archipelago during the Holocene. Series of radiocarbon datings of between 10 000 ± 40 and 2180 ± 40 years ago are evidence that the beginning of sediments accumulation, found after borehole development, is related to the Early Holocene. Diatom analysis has shown several stages in the lake development: raised bog on the border of the Pleistocene and Holocene, lagoon formation resulting from the sea level rise over 9–6 ky, and freshwater lake formation 6 ky and up to the present. Climate warming during the period attributed to the boreal and Atlantic periods of the Holocene is reflected by the dominance of Pinus pumila and Alnus serrulata assemblages in vegetation cover. Wide dune fields were formed in the Sea of Okhotsk and the Pacific shores of Paramushir Island 5–4 ky. Strengthening of atmogenic processes is related to cooling of the climate and drying of some areas of the underwater slope. Holocene Pollen Zone Northern Kuril Island Underwater Slope Gray Siltstone Anderson, P. M. aut Goryachev, N. A. aut Minyuk, P. S. aut Pakhomov, A. Yu. aut Solomatkina, T. B. aut Cherepanova, M. V. aut Enthalten in Doklady earth sciences SP MAIK Nauka/Interperiodica, 1998 430(2010), 2 vom: Feb., Seite 198-200 (DE-627)242069096 (DE-600)1422550-5 (DE-576)079718450 1028-334X nnns volume:430 year:2010 number:2 month:02 pages:198-200 https://doi.org/10.1134/S1028334X1002011X lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_70 38.00$jGeowissenschaften: Allgemeines VZ 106408305 (DE-625)106408305 38.55$jRegionale Geologie VZ 106407260 (DE-625)106407260 AR 430 2010 2 02 198-200 |
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Lozhkin, A. V. |
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550 000 VZ 38.00$jGeowissenschaften: Allgemeines bkl 38.55$jRegionale Geologie bkl First lake record of Holocene climate and vegetation change of the Northern Kuril Islands Holocene Pollen Zone Northern Kuril Island Underwater Slope Gray Siltstone |
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First lake record of Holocene climate and vegetation change of the Northern Kuril Islands |
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First lake record of Holocene climate and vegetation change of the Northern Kuril Islands |
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Lozhkin, A. V. |
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Lozhkin, A. V. Anderson, P. M. Goryachev, N. A. Minyuk, P. S. Pakhomov, A. Yu. Solomatkina, T. B. Cherepanova, M. V. |
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first lake record of holocene climate and vegetation change of the northern kuril islands |
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First lake record of Holocene climate and vegetation change of the Northern Kuril Islands |
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Abstract Investigation of Pernatoe Lake sediments in the south of Paramushir Island has enabled us to obtain the first continuous pollen record of climate and vegetation changes in the north of the Kurile archipelago during the Holocene. Series of radiocarbon datings of between 10 000 ± 40 and 2180 ± 40 years ago are evidence that the beginning of sediments accumulation, found after borehole development, is related to the Early Holocene. Diatom analysis has shown several stages in the lake development: raised bog on the border of the Pleistocene and Holocene, lagoon formation resulting from the sea level rise over 9–6 ky, and freshwater lake formation 6 ky and up to the present. Climate warming during the period attributed to the boreal and Atlantic periods of the Holocene is reflected by the dominance of Pinus pumila and Alnus serrulata assemblages in vegetation cover. Wide dune fields were formed in the Sea of Okhotsk and the Pacific shores of Paramushir Island 5–4 ky. Strengthening of atmogenic processes is related to cooling of the climate and drying of some areas of the underwater slope. © Pleiades Publishing, Ltd. 2010 |
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Abstract Investigation of Pernatoe Lake sediments in the south of Paramushir Island has enabled us to obtain the first continuous pollen record of climate and vegetation changes in the north of the Kurile archipelago during the Holocene. Series of radiocarbon datings of between 10 000 ± 40 and 2180 ± 40 years ago are evidence that the beginning of sediments accumulation, found after borehole development, is related to the Early Holocene. Diatom analysis has shown several stages in the lake development: raised bog on the border of the Pleistocene and Holocene, lagoon formation resulting from the sea level rise over 9–6 ky, and freshwater lake formation 6 ky and up to the present. Climate warming during the period attributed to the boreal and Atlantic periods of the Holocene is reflected by the dominance of Pinus pumila and Alnus serrulata assemblages in vegetation cover. Wide dune fields were formed in the Sea of Okhotsk and the Pacific shores of Paramushir Island 5–4 ky. Strengthening of atmogenic processes is related to cooling of the climate and drying of some areas of the underwater slope. © Pleiades Publishing, Ltd. 2010 |
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Abstract Investigation of Pernatoe Lake sediments in the south of Paramushir Island has enabled us to obtain the first continuous pollen record of climate and vegetation changes in the north of the Kurile archipelago during the Holocene. Series of radiocarbon datings of between 10 000 ± 40 and 2180 ± 40 years ago are evidence that the beginning of sediments accumulation, found after borehole development, is related to the Early Holocene. Diatom analysis has shown several stages in the lake development: raised bog on the border of the Pleistocene and Holocene, lagoon formation resulting from the sea level rise over 9–6 ky, and freshwater lake formation 6 ky and up to the present. Climate warming during the period attributed to the boreal and Atlantic periods of the Holocene is reflected by the dominance of Pinus pumila and Alnus serrulata assemblages in vegetation cover. Wide dune fields were formed in the Sea of Okhotsk and the Pacific shores of Paramushir Island 5–4 ky. Strengthening of atmogenic processes is related to cooling of the climate and drying of some areas of the underwater slope. © Pleiades Publishing, Ltd. 2010 |
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First lake record of Holocene climate and vegetation change of the Northern Kuril Islands |
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